
mineral
Pink corundum (ruby-bearing corundum)
Corundum, Al₂O₃; red varieties are ruby, while pink material is commonly termed pink sapphire
AI-generated identification · may be incorrectHardness 9 Mohs; vivid pink-red color, vitreous to greasy luster, trigonal crystal structure, and poor basal cleavage with conchoidal or uneven fracture. The specimen appears massive and heavily fractured, with pale matrix inclusions.
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Physical properties
Hardness 9 Mohs; vivid pink-red color, vitreous to greasy luster, trigonal crystal structure, and poor basal cleavage with conchoidal or uneven fracture. The specimen appears massive and heavily fractured, with pale matrix inclusions.
Formation & geological history
Forms through high-grade metamorphism or aluminum-rich igneous processes, commonly in marble, gneiss, or basalt-related deposits. Individual crystals may be Precambrian to younger, depending on locality.
Uses & applications
Gem-quality transparent material is cut as ruby or pink sapphire; opaque specimens are mainly collector pieces or abrasive sources. Corundum is also used industrially for abrasives and refractory ceramics.
Geological facts
Ruby’s red color is caused mainly by chromium, whereas pink corundum may contain lower chromium concentrations. Corundum is second only to diamond in natural mineral hardness.
Field identification & locations
Identify by exceptional hardness, strong color, nonmetallic luster, and lack of prominent cleavage; ruby commonly fluoresces red under long-wave UV. Important localities include Myanmar, Sri Lanka, Madagascar, Mozambique, and India.
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